Composition of soil water in mountain forest landscapes of the Upper Ussuri River and the estimation of export of chemical elements

N. K. Kozhevnikova, Anna G. Boldeskulvnikova, Tatyana N. Lutsenkoikova
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Abstract

This work provides new data on the concentrations and export of chemical elements with soil waters of various plant communities of slope and valley- fl oodplain landscapes in the basin of upper reaches of the Ussuri River. The data show that the most nutrient-rich waters are formed in humus horizons of soils developed under elm-ash communities of valley- fl oodplain landscapes. More than 80% of the content of these elements are accumulated in the soil profi le and support the functioning of communities. The waters of humus horizons of valley- fl oodplain communities are a potential source of elements entering river waters during periods of maximum precipitation. Soil waters of the mineral horizons of slope under mixed coniferousdeciduous communities are more acidic and transport relatively high amounts of dissolved organic carbon, iron, aluminum and phosphorus.
乌苏里江上游山地森林景观土壤水分组成及化学元素输出估算
本研究为乌苏里江上游流域坡地和河谷泛洪平原不同植物群落土壤水分中化学元素的富集和输出提供了新的数据。数据表明,最富营养的水形成于河谷-洪泛平原榆树群落下发育的土壤腐殖质层。这些元素的80%以上的含量在土壤剖面中积累,并支持社区的功能。在最大降水期,河谷-洪泛平原群落的腐殖质层水是进入河流水体的潜在元素来源。针叶林-落叶混交群落坡面矿质层土壤水分酸性更强,溶解有机碳、铁、铝、磷输运量相对较高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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